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单个无机和有机亚微米级液体颗粒的湿度依赖性表面张力测量

Humidity-dependent surface tension measurements of individual inorganic and organic submicrometre liquid particles.

作者信息

Morris Holly S, Grassian Vicki H, Tivanski Alexei V

机构信息

Department of Chemistry , University of Iowa , Iowa City , Iowa 52242 , USA . Email:

出版信息

Chem Sci. 2015 May 1;6(5):3242-3247. doi: 10.1039/c4sc03716b. Epub 2015 Mar 31.

Abstract

Surface tension, an important property of liquids, is easily measured for bulk samples. However, for droplets smaller than one micron in size, there are currently no reported measurements. In this study, atomic force microscopy (AFM) and force spectroscopy have been utilized to measure surface tension of individual submicron sized droplets at ambient pressure and controlled relative humidity (RH). Since the surface tension of atmospheric aerosols is a key factor in understanding aerosol climate effects, three atmospherically relevant systems (NaCl, malonic and glutaric acids) were studied. Single particle AFM measurements were successfully implemented in measuring the surface tension of deliquesced particles on the order of 200 to 500 nm in diameter. Deliquesced particles continuously uptake water at high RH, which changes the concentration and surface tension of the droplets. Therefore, surface tension as a function of RH was measured. AFM based surface tension measurements are close to predicted values based on bulk measurements and activities of these three chemical systems. Non-ideal behaviour in concentrated organic acid droplets is thought to be important and the reason for differences observed between bulk solution predictions and AFM data. Consequently, these measurements are crucial in order to improve atmospheric climate models as direct measurements hitherto have been previously inaccessible due to instrument limitations.

摘要

表面张力是液体的一项重要特性,对于大量样本而言很容易测量。然而,对于尺寸小于一微米的液滴,目前尚无相关测量报道。在本研究中,原子力显微镜(AFM)和力谱技术被用于在环境压力和可控相对湿度(RH)条件下测量单个亚微米级液滴的表面张力。由于大气气溶胶的表面张力是理解气溶胶气候效应的关键因素,因此研究了三种与大气相关的体系(氯化钠、丙二酸和戊二酸)。成功实现了单颗粒原子力显微镜测量直径约200至500纳米的潮解颗粒的表面张力。潮解颗粒在高相对湿度下持续吸水,这会改变液滴的浓度和表面张力。因此,测量了表面张力随相对湿度的变化。基于原子力显微镜的表面张力测量结果接近基于这三种化学体系的大量测量和活度所预测的值。浓有机酸液滴中的非理想行为被认为很重要,这也是在大量溶液预测和原子力显微镜数据之间观察到差异的原因。因此,这些测量对于改进大气气候模型至关重要,因为由于仪器限制,此前一直无法进行直接测量。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fa07/5490419/ed8f488d753e/c4sc03716b-f1.jpg

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